“…Latitudinal changes in NAP phytoplankton biomass have been recorded and attributed to regional climate patterns reflected by a progressive warming towards the southern end of the Peninsula, with increasing chlorophyll‐ a in that sector, contrasting with trends recorded northwards (Brown et al, 2019; Montes‐Hugo et al, 2009). Moreover, these changes in phytoplankton biomass have been followed by shifts in community composition, particularly resulting in a smaller fraction of large diatoms in the northern sector (Bahlai et al, 2021; Brown et al, 2019; Montes‐Hugo et al, 2009; Schofield et al, 2010). In the NAP region, specifically, several studies have reported an increasing contribution of small cryptophytes to the phytoplankton community composition (e.g., Mendes et al, 2013; Mendes, Tavano, Dotto, et al, 2018; Mendes, Tavano, Kerr, et al, 2018), with our decadal in situ dataset suggesting a niche segregation between cryptophytes and diatoms based on physical and chemical properties of the water‐column (Figure S2).…”